THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA

and hurricanes according to the Saffir- Simpson scale. Among of these, there existed three outstanding huge hurricanes, Katrina, Rita and Wilma with surface wind more than 150 Knots. The present paper investigates the role played by the blocking system over the northern hemisphere on hurricane Katri...

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Main Author: Yehia Hafez
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4284
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.534.4284 2023-05-15T17:30:07+02:00 THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA Yehia Hafez The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4284 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4284 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://ams.confex.com/ams/pdfpapers/127810.pdf text ftciteseerx 2016-01-08T10:45:14Z and hurricanes according to the Saffir- Simpson scale. Among of these, there existed three outstanding huge hurricanes, Katrina, Rita and Wilma with surface wind more than 150 Knots. The present paper investigates the role played by the blocking system over the northern hemisphere on hurricane Katrina. The 6- hour and daily NCEP/NCAR reanalysis data composites for the meteorological elements (surface pressure, surface wind, precipitation rate and geopotential height at 500 mb level) over the northern hemisphere for August 2005 has been used through this study. In addition to that, satellite images for hurricane Katrina and its hazards have been used. These datasets have been analyzed using of anomalies methodology. The results revealed that there existed a diffluent block persisted over Siberia and associated with a huge westerly air current aloft over the north America from 22 to 31 August 2005. Also, a strong westerlies air current aloft existed over the north Atlantic region. Splitting of westerlies occurred over the north Atlantic and it has two appreciable branches. First one goes toward the north and the second one to the south direction toward of the tropical Atlantic region. The splitting of main air current over the north Atlantic exist an unusual strong north east and easterly wind in the tropical Atlantic region. These unusual winds that caused by the blocking system in the northern hemisphere circulate, accelerate and control the track of hurricane Katrina from 23 to 31 August 2005. Whereas, analysis of the 10- day mean anomaly of the geopotential height at 500 mb for the northern hemisphere for August month of 2005 year revealed that there is an outstanding positive anomalies more than + 200 m over the north America simultaneously with positive anomalies more than + 150 m over Siberia occurred only during the last 10 days of August 2005. 1. Text North Atlantic Siberia Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description and hurricanes according to the Saffir- Simpson scale. Among of these, there existed three outstanding huge hurricanes, Katrina, Rita and Wilma with surface wind more than 150 Knots. The present paper investigates the role played by the blocking system over the northern hemisphere on hurricane Katrina. The 6- hour and daily NCEP/NCAR reanalysis data composites for the meteorological elements (surface pressure, surface wind, precipitation rate and geopotential height at 500 mb level) over the northern hemisphere for August 2005 has been used through this study. In addition to that, satellite images for hurricane Katrina and its hazards have been used. These datasets have been analyzed using of anomalies methodology. The results revealed that there existed a diffluent block persisted over Siberia and associated with a huge westerly air current aloft over the north America from 22 to 31 August 2005. Also, a strong westerlies air current aloft existed over the north Atlantic region. Splitting of westerlies occurred over the north Atlantic and it has two appreciable branches. First one goes toward the north and the second one to the south direction toward of the tropical Atlantic region. The splitting of main air current over the north Atlantic exist an unusual strong north east and easterly wind in the tropical Atlantic region. These unusual winds that caused by the blocking system in the northern hemisphere circulate, accelerate and control the track of hurricane Katrina from 23 to 31 August 2005. Whereas, analysis of the 10- day mean anomaly of the geopotential height at 500 mb for the northern hemisphere for August month of 2005 year revealed that there is an outstanding positive anomalies more than + 200 m over the north America simultaneously with positive anomalies more than + 150 m over Siberia occurred only during the last 10 days of August 2005. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Yehia Hafez
spellingShingle Yehia Hafez
THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
author_facet Yehia Hafez
author_sort Yehia Hafez
title THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
title_short THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
title_full THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
title_fullStr THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
title_full_unstemmed THE ROLE PLAYED BY BLOCKING OVER THE NORTHERN J P 3.51 HEMISPHERE ON HURRICANE KATRINA
title_sort role played by blocking over the northern j p 3.51 hemisphere on hurricane katrina
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4284
genre North Atlantic
Siberia
genre_facet North Atlantic
Siberia
op_source https://ams.confex.com/ams/pdfpapers/127810.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.4284
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